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Open AccessJournal ArticleDOI

Reflections on O2 as a Biosignature in Exoplanetary Atmospheres.

Victoria S. Meadows
- 01 Oct 2017 - 
- Vol. 17, Iss: 10, pp 1022-1052
TLDR
Environmental factors for abiotic O2 have been identified and will improve the ability to choose optimal targets and measurements to guard against false positives, and thorough evaluation of potential biosignatures works to increase confidence in life detection.
Abstract
Oxygenic photosynthesis is Earth's dominant metabolism, having evolved to harvest the largest expected energy source at the surface of most terrestrial habitable zone planets. Using CO2 and H2O—molecules that are expected to be abundant and widespread on habitable terrestrial planets—oxygenic photosynthesis is plausible as a significant planetary process with a global impact. Photosynthetic O2 has long been considered particularly robust as a sign of life on a habitable exoplanet, due to the lack of known “false positives”—geological or photochemical processes that could also produce large quantities of stable O2. O2 has other advantages as a biosignature, including its high abundance and uniform distribution throughout the atmospheric column and its distinct, strong absorption in the visible and near-infrared. However, recent modeling work has shown that false positives for abundant oxygen or ozone could be produced by abiotic mechanisms, including photochemistry and atmospheric escape. Environm...

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Evolved Climates and Observational Discriminants for the TRAPPIST-1 Planetary System

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References
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Journal ArticleDOI

Abiotic Ozone and Oxygen in Atmospheres Similar to Prebiotic Earth

TL;DR: In this paper, an altitude-dependent photochemical model with the enhanced lower boundary conditions necessary to carefully explore abiotic O 2 and O 3 production on lifeless planets with a wide variety of volcanic gas fluxes and stellar energy distributions is presented.
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Hydrodynamic Escape of Oxygen from Primitive Atmospheres: Applications to the Cases of Venus and Mars

TL;DR: In this paper, it was shown that oxygen produced by photodissociation of water vapor in an earlier stage of terrestrial planet evolution may be lost by hydrodynamic escape, although in relatively modest amounts.
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Biomarkers from Huronian oil-bearing fluid inclusions: An uncontaminated record of life before the Great Oxidation Event

TL;DR: The authors reported detailed molecular geochemistry of oil-bearing fluid inclusions from a ca. 2.45 Ga fluvial metaconglomerate of the Matinenda Formation at Elliot Lake, Canada.
Journal ArticleDOI

Maximizing the ExoEarth Candidate Yield from a Future Direct Imaging Mission

TL;DR: In this paper, a method called Altruistic Yield Optimization was proposed to estimate exoEarth candidate yield for a large suite of mission and astrophysical parameters using single visit completeness.
Journal ArticleDOI

Detecting and constraining n2 abundances in planetary atmospheres using collisional pairs

TL;DR: In this article, the authors used radiative transfer models to generate synthetic emission and transit transmission spectra of self-consistent N2-CO2-H2O atmospheres, and analytic N2H2 and N2CO2−CO2 atmospheres.
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